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Thermal evolution of high-pressure metamorphic rocks in the Alps
F.M. Brouwer
Department of Earth Sciences Utrecht (DES / IVAU)
Structural geology and EM
Structural geology & tectonics
Research output
:
Thesis
›
Doctoral thesis 1 (Research UU / Graduation UU)
Overview
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Dive into the research topics of 'Thermal evolution of high-pressure metamorphic rocks in the Alps'. Together they form a unique fingerprint.
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Keyphrases
Numerical Modeling
100%
Possible Causes
100%
Thermal Evolution
100%
High-pressure Rocks
100%
High-pressure Metamorphic Rocks
100%
High Pressure
50%
Earth Surface
50%
Central Alps
50%
Metamorphism
50%
Geological Evidence
50%
Unresolved Issues
50%
Pressure-temperature
50%
Process Modeling
50%
High-pressure Metamorphism
50%
Field-based Studies
50%
Metamorphic Evolution
50%
Pressure-temperature-time Path
50%
Time Trajectories
50%
Internal Zone
50%
Rock Modeling
50%
Very High Pressure
50%
Alpine Geomorphology
50%
Modeling Results
50%
Earth and Planetary Sciences
Exhumation
100%
Thermal Evolution
100%
Metamorphic Rock
100%
Numerical Modeling
66%
Geology
33%
Earth Surface
33%